Method and apparatus for logging boreholes



v INVENTOR. HUBERT GuYoa.

ffwm H. GUYOD Sept. 30, 1947.

lMETHOD AND APPARATUS FOR LOGGING BOREHOLES 2 Sheets-Sheet 2 Filed April 19, 1943 m @Y mu ,Ww LR @fome-p1 t The pr sen invention comprehends both methd andft-apparatus for logging wells but with a wie Patented Sept. 30, 1947 Manson AND APPARATUS Fon Loccnva nonnnouis Hubert Guyod, Houston, Tex.

Application April 19, 1943, Serial No. 483,578-

'I'his invention relates to method and 'apparatus for logging wells and pertains more particu- --lai'ly to the determination of the degree of -anisotropy and other. non-homogeneities of the beds penetrated by the well bore.

The invention' relates to and broadly comprehends tljielsubiect` matter ol* my copending but A'now abndonedlapplication, SerialvNo. 329,22*?,4 Y filed April 12,1940.' for Method and apparatus for logging bore holes-'and this application is a continuation in as to my application Serial No. 333,486, rfiled May 6, 1940, and laterabandoned. ijfownthat stratiiled earth formations lredpdiiierences in electrical charac- Herent directions relative to the bediaticuiar view of locating isotropic and/or anisotropic formations and determining the various i f'signiiicant features of such formations.

.o The primary obj-ect of the invention is to provide methodl and-apparatus for determining the g location, naturefand-fe trated by a well bore.v v

e'nt of formations pene- Another object ist ioprovide infomation on haiisotropic formations penetrated by the 'well' Still another object is tc provide infomation' on non-homogeneities in the beds penetrated by the .well bore.

Still another object is to establish an electrical disturbance about the well bore and ,to measure the variations within the area ofthe disturb- :nce as an indication of the anisotropicV condiion. f f

Another object is to establish electrical conditions in and about a'well bore by avariable magneti'oseid meneame-ng the variations in the electrical conditionslin, the area of current conduo-'tion yas vsuoli area is-.made to traverse tno wen .The foregoing obiectstogether with others will be' apparent. from-tho, following ldescription taken in connecti'onwiththe accompanying drawingsin v f Fig. 1 is adiagrainmatio illustration of a well bore penetrating-earth formations, an illustrative embodiment of apparatus of the invention beingshowni` Fig. 2 is a top view of the coils used in one form of apparatus according to the invention;

Figs. 3 and @are graphical illustrations of re- 3 Claims. .(01.175-1820 iults obtainable in thepractice -ffrthe'inven- OmU Fig, 5 illustrates a modined'form' ofenergizing In Fig. l there is shown a vertical bore I which penetrates isotropic formations 'land- 3 interspersed by an anisotropic bedded formation '4 making an angle a with the horizontal. The

' illustrative embodiment of apparatus shown in 1o Fig. 1 4comprises a source of magnetic iiux which is shown schematically as two identical L-shaped iron core coils B and l. The longer arms of these coils are placed close together and are parallel to the axis oi the bore hole. The shorter arms I and 8 make an angle of 90 with each other in a horizontal plane as shown vin Fig. 2 which is a top view of the coils. These coils are connected by means ofconductors I and i0, and Il and l2 to a two phase generator I3 located at the surface, nearthe mouth of the well.

The two alternating currents ilowing respectively, in the coils are sinusoidal and one of them is 90 out of phase with the other. Their intensities are read on two 4meters lI4 and I5, and 2o are maintained equal ineach circuit by means of a rheostat Il. The frequency ,will be oi at least 100 cycles. xAn electrode l1, preferably of the'non-polariz'- ing type, is located within the well bore at a short iixed distance-2 feet for instance-above the coils, 'and is connected by means loi conductor I8v to an oscillograph Il located'atjthe surface and whose other terminal is grounded at 20.

The conductor il is provided with aagrounded magnetic shield 2i, so that there will beno current induced into 'circuit i1, Il, 20 from the power conductors s." l0, l I, i 2.

The potential difieience between electrodes il and 20 might be relatively small and itis understood that the oscillcmph i! will include such instrumentalities' as necessary, so that the desired amplitude of indication .will be obtained.

Coils l and l are mounted in a non-conducting andnon-magnetic case, so as to make a singie unit 22 which can be lowered inside the bore hole at the end of the conductors which, for the to the high permcance of the core of the coils,

' moet of' the magnetic flux of each coil follows the core withlittle or no magnetic loss at the bends.

In order .to better visualize the behavior ofthe total magnetic held .existing in the vicinity o f the electrode i1, the amplitude and-direction of this held at av-iew be' first conpumose can be 4assembled as a single cable. Due

sidered. The magnetic iield leaving .one oi the extrer'nlties oi' a coil, for instance the arm 1 of coil 5, comprises a plurality `o! lines oi' tlux. For the sake of simplicity itis convenient to suppose that at this pole the eiiect o! all of the lines of flux would be the same as li' only one line existed. the intensity of such line being equal to the total flux at this point. Hereaiter this line will be termed mean magnetic flux. By reason of symmetry, this mean magnetic flux is oriented along the axis of the arm 1. Similar consideration can be made regarding the ux near the extremity of the arm l.

At a given instant, t, the magnitude ci the mean magnetic nux at the upper and lower extremities of the coil l can be represented by horizontal vector 23 (Fig. 2) and vertical vector 24 phase relation-and value of currents. the length of the respective vectors is: 1'

Vector 23= C sin (Zrft-i-d) 'vetto'i- 21aasin (21m-5H)- vector 24=c' sin (21m-a) vVector v26=C" sin Where C and Cf are constants related irrparticular to the details of the core form an'dtothe root-meanfsquare current in the coils, which current is assumedl to be several amperes; 4 is the phase angle of the mean ux 23; and l is the frequency oi the electric current energizing the coils.

To better visualize the operation oi'` the method, simplification is had in the following disclosure -by assuming that the length of the respective arms l and 8 is small enough that the origin of the vectors 23 and 25 canbe considered as located at the point 2l, the intersection o! the axes of the two arms. Vectors 23 and 2l are at right angles to each other by virtue ot the orientation of the magnetizable members which include the pole pieces 1 and 8. This is illustrated in Fig. 2 of the drawings. The vectors 22 and 25 can be vectorially added and the vector sum thereof is the vector 21 which is of constant length and which is rotating at a constant velocity in the horizontal plane of l and 8, it being assumed that the excitation of the coils 5 and i is equal.

Also for the sake of simplicity it will be assumed that the vectors 24 and 2B, which are par allel and close together, can be replaced by a single vertical vector 28 which may be assumed as being located on the axis of the instrument 22. The length of this vector is:

cfs/itin (2111+ :1l-H.)

It is known that when a magnetic ileld varies in direction or intensity in a conducting medium, eddy currents and consequently potential-changes will be produced in the medium. It is also known that the formations traversedby a bore hole are usually conductive to electric current. It is therefore apparent that when the coils i and 8 are energized, the variable magnetic ilux represented by the resultant of vectors 21 and 28 will induce electric currents and potential changes which can be picked up by electrode I1. The other electrode 20 will usually be so far from the unit 22 that the variations of potential in its vicinity are negligible, and the potential o! this electrode can be used as a reference for the potential measurements.

If the vertical arms o! the coils are made long enough-20 feet or more, for instancethe iniiuenceoi the magnetic ilux 28 on electrode I1 will be `quite Smau, and we will assume thatv 1t is A. as a whole around the axis of the instrument. To

Simplify theV Wording, We shall refer to these groups of ilux lines as the vertical and horizontal ilelds respectively. With the assumption made v,oi electrode l1.

' Itis apparent that the above description of the behavior oi' the magnetic field has been simplinedsomewhat and that, quantitatively, the results arrived at are not fully exact. It will be sp1 ground, that is to say, the potential which could be measured when no artificial current flows inthe ground. Second: the potential changes created by the current induced in the ground by the horizontal ileld. i

Other potentials may also exist, like electrode polarization, stray current potential, etc.. but it is assumed that those expert in the art of well logging are aware of them and have knowledge to suppress them or take them into consideration in the interpretation of the result, i! necessary.

It is` presumed rst that the instrument is motionless in the hole so that the natural potential will then be constant. In a homogeneous formation, or in a horizontally bedded !orma-' tion, the eilect of the horizontally rotating field on electrode i1 will be approximately constant, regardless o! the angular position of the. iield. Therefore, the potential diii'erence, V, between the potential electrode l1 and the ground electrode 20 is approximately constant. In polar coordinates, the magnitude of this potential diierence can be represented by a circular iigure 30-1 see Fig. 3which is almost a. perfect circle, whose center is Il, pole of the coordinate system. The polar angle at any instant is (Zrft-l-) 0 being the lphase angle between the V and the inducing curtween the major and the minor axes of the diawhere gram l2.

and its center 33 does not nec- 1 Local non-homogeneities can also change the shape or size of the closed figure, for instance, changes in the size of the bore hole, variations of conductivity, etc., so that sometimes the result will be related to several physical changes in or close tothe formations to be logged.

When the apparatus is made to travel in the .bore hole, the potential of electrode I1 will vary, and the varying potential can be plotted in terms of depths in the form of an electric log.`

In the case of the formations assumed on Fig. 1, the electric log would be as illustrated on Fig. 4 curve 34 shows the potential changes 'measured without energizing the coils; curve Il shows the potential changes due solely to the artiflcial current induced in theground; and curve 38 represents the total potential changes. Of

course, it will usually be impossible to obtain directly curve 35, but by making two 'sets of meas-` urements, one without and one with the energizing current, curves 34 and 36 will be registered respectively; curve 35 can then be obtained by subtracting curve 34 from curve 3C. In many instances this subtracting will not/be necessary, because curve 36 will give all the desired information.

It can be readily understood that in many cases 4vthe study of curve 35 will allow evaluating apA proximately instance, an almost straight good isotropy,

the part played by each factor. For curve will indicate a whereas wiggles of the same frequ/ncy as that of the generator I3 will indicate anisotropy. Changes in the average potential value will be related to changes in the conductivity of the formations, etc.

If the .currents used toenergize coils l and! l are not sinusoidal, or if their phase anglais different from 90, the intensity and/or the angular velocity of the horizontal field 21 will vary. If f the vertical arms of the coilsare short or totally 6 placed by one or several rotating permanent magnets, and that similar results will be obtained.

It will be appreciated that the generator I! can be located inside of the unit 22, and energized either by storage batteries located also in the unit, or from the surface by means of a single conductor. This procedure has the advantage of eliminating a number of conductors between unit 22 and the surface.

Although the use of two coils with independent cores has beeny mentioned above, it y is of course possible to wind the two coils on a single core unit having two horizontal arms and one vertical arm. f

The modification in apparatus as illustrated in Fig. relies upon variations in transformer action, and 31 is a constant voltage two'phaso generator, the phase angle being 90. It is un-v derstood that the current flowing in coils 5. and i induces currents in the surroundingformations. These induced currents in turn induce a counterelectromotive force in the coils so that the difierence between the applied potential and such counter-electromotive force is instrumental in causing current to flow in the coils l and l. The counter-electromotive force in the respective coils depends uponv the nature of the formations angularly with respect to these coils and hence the', difference in the readings of the instruments Il and i6 in conductors 9 and I2 is indicative of/the l location, extent of anisotropy and/or non-homogeneity of the traversed formations.

While the foregoing disclosure refers to specific examples of procdure and apparatus it is to be understood that the present invention is not con- `fined to such'speciflc techniques and devices.

Broadly the invention comprehends method land apparatus for logging wells. if lWhat is claimed is: Y

1. The method of logging geological formations traversed by a well bore comprising the steps of, subjecting an area about the well bore to a magnetic ux rotating in a predetermined plane and at such a rate that induced currents are created by the rotating flux in conducting formations adjacent to the w/ell bore, and simultaneously measuring within said area the variations in the potential, resulting from the currents induced in the formations, as an indication ofthe gnisotrpy of the strata penetrated by the well ore.

2. Apparatus for determining anisotropy of strata penetrated by well bores comprising a plussrality of elongated magnetizable members havabsent, or if the two coils are not identical, or

if more coils are used, the horizontal and ver It seems apparent that the coils can be re- 'l5 ing outwardly extending and angularly spaced pole pieces thereon, magnetizing coils for said members, a source of polyphase current connected to said coils, the ends ofsaid members opposite tical fields will be different from those heretothe pole pieces being displaced from the pole tential at a point within the area of currentyconductions/f I 3.' Apparatus for determining anisotropyv of strata penetrated by a bore hole comprising, a

source of magnetic ilux to be lowered into the bore hole, saidl source including magnetized means comprising a plurality of elongated magnetizable members having outwardly extending and angularly spaced pole pieces, meansfor so energizing said members as to produce a rotating magnetic aux to induce currents in conducting'form# tions adjacent to the well` bore, and means ifor determining'=.the variations in the current pattern in varlos strato as an indication of the anisotropy or a penetrated formation.

o HUBERT Guyon.

l nmnmcns crrnn The following references' are ot record in the '111e of thispatent:

Number 1,805,900 2,139,460

UNIIED'BI'ATES lI-'A'I'EN'IS Name l Dato .Ambronn May 19,1931 Potapenko Dec. 6, 1938 Athy Apr. 30,1940 Jakosky Aug. 13. 1940 Athy Nov. 11-,- 1941 Pearson et nl. Feb. 321942 Zuschlag Apr. '1,1942 

